共查询到20条相似文献，搜索用时 109 毫秒
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破坏性地震发生后,传统的地面通信网络会受到严重的破坏,甚至会处于瘫痪状态,无法保证前后方应急指挥部之间的数据传输、应急通信、指挥调度等应急需求。为了确保地震应急指挥的顺利开展,需要有一套安全、可靠的通信系统,而我国自主研制的北斗卫星导航系统（BDS）是全球性的卫星导航系统,具有精准定位导航、精密授时、短报文通信等功能,可以在灾害应急指挥中发挥重要作用。因此,从地震现场应急工作的需求出发,在分析各种通信技术的基础上,研究探索一种基于北斗卫星导航系统的地震应急现场通信系统,以满足快速获取灾情信息、精准定位灾区位置、实时传送灾情报告的地震现场应急需求,保障地震现场通信能够畅通无阻,确保应急指挥顺利开展。 相似文献
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青岛市地震应急指挥决策支持软件的设计与开发 总被引：1，自引：0，他引：1
基于空间决策支持技术设计与开发了城市地震应急指挥决策支持软件,在软件的总体设计、功能模块、数据库建设、接口设计与模块集成等方面进行了研究与开发,并在青岛市地震应急指挥系统中得到实际应用和检验。实践表明,该软件能实时收集地震现场灾害信息,给出地震灾害现状图,并且实时跟踪灾情发展及变化,智能制定各种地震应急指挥指令,可视化绘出应急指挥决策图,从而有效提高地震应急指挥的效率和响应速度,为地震现场应急指挥工作提供了更实用、可推广的技术平台,这对全国大中城市地震应急指挥技术系统的建设具有实际意义。 相似文献
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福建省地震现场应急通信系统是一个集现场通信与传输、信息获取与处理、现场指挥、后勤保障于一体的地震现场流动应急指挥系统.在中国地震局的统一部署下,经过“福建省数字地震观测网络”项目建设,该系统已经成为“中国数字地震观测网络”的重要组成部分. 相似文献
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地震应急是我国防震减灾工作3大体系之一,鉴于地震预报尚不过关,在没有作出临震预报而地震突然发生时,为在灾区进行有效的救援而采取的紧急行动.通信、计算机等新技术是地震应急指挥和救援工作顺利进行的重要保证,无线局域网是计算机网络与无线通信技术相结合的产物,无线局域网利用了无线多址信道的一种有效方法来支持计算机之间的通信,本文根据新疆地震局地震应急现场工作情况,阐述无线局域网在地震应急现场中的应用,讨论了地震应急现场所适应的几种无线局域网的组网模式. 相似文献
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国家地震应急指挥技术系统建设中的关键技术及应用 总被引：5，自引：4，他引：1
地震应急指挥系统是国家公共安全平台的一个重要组成部分,同时也是地震应急指挥技术系统为国家与各级地方政府进行地震应急指挥服务的专业技术支持系统。本文以数字观测网络项目为背景,全面归纳和总结了国家地震应急指挥技术系统建设中的关键技术及具体应用。 相似文献
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介绍了广东省地震应急指挥技术系统是为广东省抗震救灾指挥部实施地震应急救援指挥提供技术支撑的系统,系统主要由四部分构成:地震应急指挥通信、震灾快速评估与辅助决策、地震灾情速报。提出系统为实现地震应急信息快速传递、处理,提高应急救灾指挥与决策的技术水平,最大限度地减少震时的混乱和人员伤亡,提供了高效的指挥技术平台。并对广东省地震应急工作提出展望。 相似文献
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The determination of the coefficient of viscosity of eruptive products gives useful elements to the knowledge of possible variations of composition and physical conditions of the magmas. 相似文献
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As is known, the secular deceleration of the Earth's diurnal rotation is explained mainly by the tidal friction in the ocean. Below we consider this mechanism in some detail, taking into account also elastic deformations of the mantle under the action of ocean loading and the interaction between the tide-generating body, ocean tidal wave, liquid outer core, and solid inner core. It is shown that elastic displacements of the core-mantle boundary under the action of ocean loading are of about the same amplitude and phase as the elastic loading displacements of the Earth's outer surface. As a result, side by side with the mechanism of secular deceleration of diurnal rotation of the mantle, there are also (1) the opposite mechanism of secular acceleration of diurnal rotation of the outer liquid core and of the solid inner core and (2) the mechanism of excitation of differential rotation in the liquid core. Taking these effects into account, we compare theoretical and modern observed data on the eastward drift of the solid inner core. It is shown that the best agreement may be obtained if the turbulent viscosity of the liquid core is about 2 × 10
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Poise 相似文献
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The nutations of the planets Mars andEarth are investigated and compared. Alarge number of interior structureparameters are involved in the nutationcomputations. The comparison between the observations and the computationsprovides several constraints on these parmeters andtherefore allows a better understanding of the physics of the interior of theplanet. For the Earth, the high precision of the observations of the nutationshas led to a very good determination of interior properties of the planet. ForMars, observations of nutations are not yet available, and we review how theamplitude of the Martian nutations depends on the hypotheses consideredfor its interior. Although Mars is very similar to the Earth, its interior is not well known;for example, we don't knowif its core is liquid or solid. Only if the core is liquid,the Free Core Nutation (FCN) normal mode exists and can alter the nutationswhich are close to the resonance. From the observed geoids, it is known thatboth planets are not in hydrostatic equilibrium. The departure is larger forMars than for the Earth, and consequently, the implication of considering a convective mantle instead of a mantle in hydrostatic equilibrium described byClairaut's equation for the initial equilibrium state of the planet is largeron the Martian nutations than on the Earth nutations. The consequences of theuncertainty in the core dimensions are also examined and shown to be of a veryhigh influence for Mars if the core is liquid, due to the potential changes inthe FCN resonance. The influence of the presence of an inner core, which isknown to exist for the Earth, could be more important for Mars than for theEarth if the inner core is large. Due to the presence of Tharsis on Mars, thetriaxiality of this planet has, additionally, larger effects than on Earth. 相似文献
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Studia Geophysica et Geodaetica - 相似文献
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地震激励下处于深水中的桥墩和周围水体的相互作用将对桥梁结构的动力响应产生较大影响。首先对地震作用下水-桥墩的相互作用理论做了概括,给出了动水压力对桥墩的作用效应及各自的适用范围;对主要的三种考虑流固耦合效应的分析方法做了对比,探讨了地震作用下影响水-结构相互作用的主要因素,并对今后的研究提出了建议。 相似文献
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Geomagnetism and Aeronomy - The magnetic evolution of the active region of the Sun at the level of the photosphere has been studied. Magnetic synoptic maps of the 2007 Kitt Peak Observatory were... 相似文献
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V. E. Pavlov T. Yu. Tolmacheva R. V. Veselovskiy A. V. Latyshev A. M. Fetisova I. V. Bigun 《Izvestiya Physics of the Solid Earth》2017,53(5):702-713
Until recently, the existing data prevented the geophysicists from accurately dating the Bysy-Yuryakh stratum, which outcrops in the middle reach of the Kotuy River, constraining the time of its formation to a wide interval from the end of the Late Cambrian to the beginning of the Silurian. The obtained paleomagnetic data unambiguously correlate the Bysy-Yuryakh stratum to the Nyaian regional stage and constrain its formation, at least a considerable part of it, by the Tremadocian. This result perfectly agrees with the data on the Bysy-Yuryakh conodonts studied in this work and yields a spectacular example of the successful application of paleomagnetic studies in solving important tasks of stratigraphy and, correspondingly, petroleum geology. Within the Bysy-Yuryakh stratum, we revealed a large normal-polarity interval corresponding to the long (>1 Ma) period when the geomagnetic reversals were absent. This result, in combination with the data for the Tremadocian and Middle–Upper Cambrian sequences of the other regions, indicates that (1) the rate of occurrence of the geomagnetic reversals on the eve of the Ordovician Moyero superchron of reversed polarity was at most one reversal per Ma; (2) the superchron does not switch on instantaneously but is preceded by a certain gradual change in the operation conditions of the dynamo mechanism which, inter alia, manifests itself by the reduction of the frequency of geomagnetic reversals with the approach of the superchron. This finding supports the views according to which a process preparing the establishment of the superchrons takes place at the core–mantle boundary. 相似文献
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Ivanka Jakubcová Věra Marvanová Miloš Pick Antonín Novotný Reviewer Z. Šimon 《Studia Geophysica et Geodaetica》1982,26(2):193-196
Summary The results of two different methods of the determination of the non-linearity of the gravimeter scale are compared; the economy is discussed as well. 相似文献